Kamb Ice Stream

Results: 13



#Item
1and rotation is slowed or stopped by recrystallization. In general on ice sheets, divergent flow causes C axes to cluster symmetrically about the vertical axis, parallel flow causes C axes to cluster about the vertical a

and rotation is slowed or stopped by recrystallization. In general on ice sheets, divergent flow causes C axes to cluster symmetrically about the vertical axis, parallel flow causes C axes to cluster about the vertical a

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 07:07:54
2The purpose is to register the image as to its precise location and scale and to quantify the size of features that appear on the images. From Byrd Station, we cooperated with R. Bindschadler (National Aeronautics and Sp

The purpose is to register the image as to its precise location and scale and to quantify the size of features that appear on the images. From Byrd Station, we cooperated with R. Bindschadler (National Aeronautics and Sp

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 16:45:14
3wires at the same site. The different trends during this period are partially due to transient effects, but these effects tend to diminish with time. The difference may be primarily due to crevassing or other inhomogenei

wires at the same site. The different trends during this period are partially due to transient effects, but these effects tend to diminish with time. The difference may be primarily due to crevassing or other inhomogenei

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 21:19:52
4Further data analysis will be a cooperative project involving both institutions. Jerry Bradley (USGS, Denver), Tom Grover (USGS, Denver), Bruce Vaughn (USGS, Tacoma), and Kurt Hayden (Ohio State University) participated

Further data analysis will be a cooperative project involving both institutions. Jerry Bradley (USGS, Denver), Tom Grover (USGS, Denver), Bruce Vaughn (USGS, Tacoma), and Kurt Hayden (Ohio State University) participated

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 16:45:24
5References Interpretation is still in progress, but preliminary results indicate that the heating rate implies high shear stress, high enough to be important in the force balance of the ice stream as predicted. A quanti

References Interpretation is still in progress, but preliminary results indicate that the heating rate implies high shear stress, high enough to be important in the force balance of the ice stream as predicted. A quanti

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 17:39:53
6Sticky spots under ice streams RICHARD B. ALLEY

Sticky spots under ice streams RICHARD B. ALLEY

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 19:55:11
7References Alley, R.B., D.D. Blankenship, C.R. Bentley, and S.T. RooneyDeformation of till beneath ice stream B, Antarctica. Nature, 322, 5759. Alley, R.B., D.D. Blankenship, S.T. Rooney, and C.R. Bentley. 1988.

References Alley, R.B., D.D. Blankenship, C.R. Bentley, and S.T. RooneyDeformation of till beneath ice stream B, Antarctica. Nature, 322, 5759. Alley, R.B., D.D. Blankenship, S.T. Rooney, and C.R. Bentley. 1988.

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 21:19:57
8Borehole drilling to the bed of ice stream B, Antarctica HERMANN ENGELHARDT, MARK FAHNESTOCK, NEIL HUMPHREY, and BARCLAY KAMB

Borehole drilling to the bed of ice stream B, Antarctica HERMANN ENGELHARDT, MARK FAHNESTOCK, NEIL HUMPHREY, and BARCLAY KAMB

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 16:45:29
9

PDF Document

Add to Reading List

Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 15:41:27
10Microsoft WordThird_circular_Madrid-V3bis.doc

Microsoft WordThird_circular_Madrid-V3bis.doc

Add to Reading List

Source URL: www.igsoc.org

Language: English - Date: 2008-05-28 07:18:56